|
Mitigation Option
|
Costa
|
Potential Emission Mitigationb (Mt CO2 equivalent/yr)
|
|
GEOENGINEERINGc
|
|
|
|
Low stratospheric sootd
|
Low
|
8 × 103 to
25 × 103
|
|
Low stratospheric dust-aircraft deliveryd
|
Low
|
8 × 103 to
80 × 103
|
|
Stratospheric dust (guns or balloon lift)d
|
Low
|
+
|
|
Cloud stimulated by provision of CCNe
|
Low
|
+
|
|
Stimulation of ocean biomass with ironf
|
Low to medium
|
7 × 103
|
|
Stratospheric bubbles (multiple balloons)g
|
Low to medium
|
+
|
|
Space mirrorsg
|
Low to medium
|
+
|
|
NOTE: This table summarizes the information by
source category and places the options in order of
cost-effectiveness for the Category 3 options. Cost-effectiveness
estimates are categorized as: Savings (for less than 0), Low
(0–$9/t CO2 equivalent),
Medium ($10–99/t CO2
equivalent), or High (>$100/t CO2
equivalent). The potential emission savings (which in some cases
includes not only the annual emissions, but also changes in
atmospheric concentrations already in the atmosphere) for the
geoengineering options are also shown.
|
|
aCosts are
in ranges shown below:
|
| |
$/t CO2
|
|
|
Savings
|
<0
|
|
|
Low
|
0–9
|
|
|
Medium
|
10–99
|
|
|
High
|
>100
|
|
|
bThis
number assumes that we not only mitigate the impact of current
emissions of CO2 and other
greenhouse gases, but also the stock of those gases. The CO2-equivalent emission is determined by
evaluating the equivalent reduction in radiative forcing (see
Appendix Q). These options do not reduce the flow of emissions per
se, but rather the impact of greenhouse warming from those
emissions. The ''+" indicates that there is no known physical limit
to this method assuming these options work as expected, just a
limit on the amount of mitigation for which we are willing to
pay.
|
|
cMitigation options are placed in order of
cost-effectiveness based on the average (arithmetic mean) of the
costs. Cost ranges are averaged prior to each option addition.
|
|
dThese
options cannot be considered for use until the possible effects of
the soot, dust, or aerosol on the destruction of stratospheric
ozone are understood.
|
|
eCloud
condensation nuclei.
|
|
fThis
option cannot be considered for use until the possible effects of
large-scale iron additions to the ocean biomass are well
understood.
|
|
gInfeasible options.
|